{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390282681488920064.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1186/bf03352075"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/content/pdf/10.1186/BF03352075.pdf"}},{"identifier":{"@type":"URI","@value":"https://link.springer.com/article/10.1186/BF03352075/fulltext.html"}},{"identifier":{"@type":"URI","@value":"http://link.springer.com/content/pdf/10.1186/BF03352075"}},{"identifier":{"@type":"NAID","@value":"130003956316"}}],"dc:title":[{"@language":"en","@value":"The 2000 Western Tottori Earthquake"},{"@value":"The 2000 Western Tottori Earthquake—Seismic activity revealed by the regional seismic networks—"}],"dcterms:alternative":[{"@language":"en","@value":"Seismic activity revealed by the regional seismic networks"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"On October 6, 2000, the 2000 Western Tottori Earthquake (Mjma 7.3) occurred in the western Tottori prefecture area, southwestern Japan. It initiated at a depth of 12 km at the bottom of the seismogenic zone, which was derived from aftershock distribution. The aftershocks extend over a 35 km length in a north-northwest direction. Spatial and temporal distribution of the aftershocks exhibits local characteristics in the fault region. The northern part consists of earthquake clusters while the southern part consists of a rather simple lineament of aftershocks, and the spreading and decaying rate of the aftershocks is slower in the northern part. This contrast is possibly due to the heterogeneity of the fault system and probably affected the rupture process of the mainshock. Two swarm sequences occurred in the surrounding region after the mainshock. One initiated 48 hours after the mainshock 25 km southwest of the main aftershock distribution. The other started 20 hours after the mainshock northeast of the mainshock on the southeast flank of Daisen volcano. These activities are probably induced seismicity due to stress changes in the focal region. Pre-seismic swarm activities occurred in the focal region from 1989 and deep low-frequency earthquakes were observed since 1999. It is important to understand the relationship between these possible precursory phenomena and the occurrence of the mainshock."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1420001326210308224","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"50263158"},{"@type":"NRID","@value":"1000050263158"},{"@type":"NRID","@value":"9000364793841"},{"@type":"NRID","@value":"9000283242072"},{"@type":"NRID","@value":"9000000875783"},{"@type":"NRID","@value":"9000004601797"},{"@type":"NRID","@value":"9000024114679"},{"@type":"NRID","@value":"9000009497171"},{"@type":"NRID","@value":"9000001755818"},{"@type":"NRID","@value":"9000006241018"},{"@type":"NRID","@value":"9000024132608"},{"@type":"NRID","@value":"9000254753864"},{"@type":"NRID","@value":"9000410949651"},{"@type":"NRID","@value":"9000254741330"},{"@type":"NRID","@value":"9000413261033"},{"@type":"NRID","@value":"9000254740662"},{"@type":"NRID","@value":"9000241825591"},{"@type":"NRID","@value":"9000023579024"},{"@type":"NRID","@value":"9000024127231"},{"@type":"NRID","@value":"9000001756304"},{"@type":"NRID","@value":"9000018862477"},{"@type":"NRID","@value":"9000018699100"},{"@type":"NRID","@value":"9000406386620"},{"@type":"NRID","@value":"9000279888057"},{"@type":"NRID","@value":"9000411392551"},{"@type":"NRID","@value":"9000254262851"},{"@type":"NRID","@value":"9000024112300"},{"@type":"NRID","@value":"9000311498116"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/7000008530"}],"foaf:name":[{"@language":"en","@value":"Ohmi 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Space"},{"@language":"ja","@value":"Ｅａｒｔｈ，　Ｐｌａｎｅｔｓ　ａｎｄ　Ｓｐａｃｅ"},{"@language":"en","@value":"Earth Planets Space"},{"@language":"ja","@value":"Ｅａｒｔｈ　Ｐｌａｎｅｔｓ　Ｓｐａｃｅ"}],"dc:publisher":[{"@language":"en","@value":"Society of Geomagnetism and Earth, Planetary and Space Sciences, The Seismological Society of Japan, The Volcanological Society of Japan , The Geodetic Society of Japan , The Japanese Society for Planetary Sciences"},{"@language":"ja","@value":"地球電磁気・地球惑星圏学会 、公益社団法人 日本地震学会、特定非営利活動法人 日本火山学会、日本測地学会、日本惑星科学会"}],"prism:publicationDate":"2002","prism:volume":"54","prism:number":"8","prism:startingPage":"819","prism:endingPage":"830"},"reviewed":"false","dcterms:accessRights":"http://purl.org/coar/access_right/c_abf2","url":[{"@id":"https://link.springer.com/content/pdf/10.1186/BF03352075.pdf"},{"@id":"https://link.springer.com/article/10.1186/BF03352075/fulltext.html"},{"@id":"http://link.springer.com/content/pdf/10.1186/BF03352075"}],"availableAt":"2002","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335851923328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Why do aftershocks occur? Relationship between mainshock rupture and aftershock sequence based on highly resolved hypocenter and focal mechanism distributions"}]},{"@id":"https://cir.nii.ac.jp/crid/1050564288469406080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coseismic and Postseismic Deformation of the 2016 Central Tottori Earthquake and its Slip Model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292617909532032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"New, improved version of generic mapping tools released"}]},{"@id":"https://cir.nii.ac.jp/crid/1362544420886888832","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep low‐frequency earthquakes beneath the focal region of the Mw 6.7 2000 Western Tottori earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670320399184256","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Deep, low-frequency microearthquakes in or around seismic low-velocity zones beneath active volcanoes in northeastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951794490140928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A monochromatic earthquake suggesting deep‐seated magmatic activity beneath the Izu‐Ooshima Volcano, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204305619072","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"2011年3月15日静岡県東部地震（Mj6.4）の遅れ誘発過程に関する研究"},{"@language":"en","@value":"Delayed Triggering Process for the Mj6.4 Eastern Shizuoka Earthquake of 15 March 2011"},{"@language":"ja-Kana","@value":"2011ネン 3ガツ 15ニチ シズオカケン トウブ ジシン(Mj6.4)ノ オクレ ユウハツ カテイ ニ カンスル ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206509693568","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Aftershock Distribution of the January 17, 1995 Hyogo-ken Nanbu Earthquake Determined by the JHD Method."},{"@language":"ja-Kana","@value":"Aftershock Distribution of the January"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511584896","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strong S-wave anisotropy in the aftershock region of the 2000 Tottori-ken Seibu, Japan, earthquake (MW6.6)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512889600","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The 2000 western Tottori earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681487609728","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Urgent Joint Observation of Aftershocks of the 1995 Hyogo-ken Nanbu Earthquake."},{"@language":"ja-Kana","@value":"Urgent Joint Observation of Aftershocks"},{"@value":"Japanese University Group for the urgent joint observation for the 1995 Hyogo-ken Nanbu earthquake, urgent joint observation of aftershocks of the 1995 Hyogo-ken Nanbu earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488306432","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"High resolution 3-D velocity structure in the source region of the 2000 Western Tottori Earthquake in southwestern Honshu, Japan using very dense aftershock observations"},{"@value":"High resolution 3-D velocity structure in the source region of the 2000 Western Tottori Earthquake in the southwestern Honshu, Japan using very dense aftershock observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489280768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Deep low-frequency earthquakes near the downward extension of the seismogenic fault of the 2000Western Tottori earthquake"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:0015898025"},{"@type":"CROSSREF","@value":"10.1186/bf03352075"},{"@type":"CIA","@value":"130003956316"},{"@type":"OPENAIRE","@value":"doi_dedup___::40b511a05ed080abf0c61ffc7ea83140"},{"@type":"CROSSREF","@value":"10.1186/bf03353338_references_DOI_WhlvNE0IMoKhuq2NqAa68PvgYLu"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0650-2_references_DOI_YlGsaUipnx24ptTS2bmfZb6Dobd"},{"@type":"CROSSREF","@value":"10.1029/2018jb016105_references_DOI_WhlvNE0IMoKhuq2NqAa68PvgYLu"},{"@type":"CROSSREF","@value":"10.1186/bf03351861_references_DOI_WhlvNE0IMoKhuq2NqAa68PvgYLu"},{"@type":"CROSSREF","@value":"10.1186/bf03351884_references_DOI_WhlvNE0IMoKhuq2NqAa68PvgYLu"},{"@type":"CROSSREF","@value":"10.1186/bf03352073_references_DOI_WhlvNE0IMoKhuq2NqAa68PvgYLu"},{"@type":"CROSSREF","@value":"10.4294/zisin.69.99_references_DOI_WhlvNE0IMoKhuq2NqAa68PvgYLu"}]}